Waterspout
and
funnel-cloud, as
seen from Ynyslas Beach on the morning of September
4th 2011. These
were but
two of a whole series of vortices that developed as
easterly overnight
katabatic flow off the Cambrian mountains,
caused by night-time cooling, converged with the SW
steering-flow in a
weakly unstable environment.Product
number
091129.
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